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1 se morphogen gradients, varying in range and steepness.
2 for incident waves with higher frequency and steepness.
3 instability of these waves depends on their steepness.
4 centration of PCP proteins, and the gradient steepness.
5 having different incident wave frequency and steepness.
6 smallest grains, probably contribute to the steepness.
7 tion and is accompanied by a decrease in its steepness.
8 rchical structures with different degrees of steepness.
9 ) and largest amplitude incident waves (with steepness 0.25) decayed by half over a distance of appro
11 kscatter relates to the reduction in corneal steepness after cross-linking and may become a relevant
12 ion flow rates, and optimization of gradient steepness allowed a detection limit of 4 amol, correspon
20 um cells to exponential gradients of varying steepness and local concentration of the chemoattractant
22 nction to obtain maximum conductance (gmax), steepness and midpoint potential for the voltage depende
23 ments in right eyes differed slightly in rim steepness and rim volume from those in left eyes (P < .0
25 ides a simple model that can account for the steepness and shape of F-pCa relations that other models
26 al disturbance and conversely to increase in steepness and shift towards higher TL in the case of rec
27 each participant, annual rates of BP change (steepness) and area under the BP trajectory curve (cumul
28 es of optic nerve head shape (cup depth, rim steepness, and cup size) as input into a relevance vecto
29 ates internal waves of similar amplitude and steepness as internal waves from tide-topography interac
31 der size correlates with reach-scale channel steepness but does not explain observations of highly va
32 rm of fura-2 to report [Ca2+]i, and that the steepness decreases as myofilament overlap decreases.
33 emperature strongly depended on the gradient steepness, decreasing by ~10 degrees as the steepness wa
35 ak capacity and an optimum range of gradient steepness exists in which the peak capacity is maximized
36 owever, both the total charge (Qmax) and the steepness factor (k) remained conserved at values consis
37 age, V* approximately equal to -40 to-50 mV; steepness factor, k approximately equal to 6-9 mV; holdi
38 erwise conserved maximum charge, Q(max), and steepness factor, k, in parallel with previously reporte
39 e, Qmax, the transition voltage, V*, and the steepness factor, k, of the steady-state charge-voltage
40 charge, Q(max), transition voltage, V*, and steepness factor, k, that were consistent with a persist
41 alf-maximal activating voltages (V(0.5)) and steepness factors (k), by 2 mV and 0.7, in contrast to t
43 ing parameter [Formula: see text] and of the steepness [Formula: see text] of a climatological drift
44 seen only under conditions of high gradient steepness (>10% across a typical cell length of 50 mum)
46 imensional MoS(2) channel, and obtain abrupt steepness in the turn-on characteristics and 4.5 mV deca
47 sities revealed reduced maximum currents and steepnesses in their voltage dependences after addition
48 owed a tendency to stretch (i.e. decrease of steepness), in the presence of external disturbance and
49 increased by 0.3+/-0.1% (ca. 1 K), while the steepness increased by 0.9+/-0.3% per hour of 1x10(6) cm
50 reasing chemotactic response as the gradient steepness increased from 0 to 5, 0 to 10, and 0 to 25 ng
52 s age, which, traced back to the temperature steepness index of the viscosity, tears down one of the
55 erved both the maximum charge, Qmax, and the steepness, k, of the steady-state Q(V) relationships.
56 eveal that typical local changes in seafloor steepness lead to a shallow divergence and a deep conver
60 The Hill coefficient, nH, which measures the steepness of a dose-response relationship, may be a usef
62 imal effect on channel activation, a reduced steepness of Ca(2+) dose-dependent curve, altered Ca(2+)
64 e fast and slow gates characterizing 1), the steepness of each gate's open probability on VG; 2), the
65 to 10, and 0 to 25 ng/ml, demonstrating that steepness of gradient is a major determinant of the rela
66 Recently, we identified a dichotomy in the steepness of length-tension relationships in mammalian c
67 nse times were inversely proportional to the steepness of Rac inducer gradient in agreement with a ma
69 profiles, are correlated, others such as the steepness of response profiles, are set independently.
70 ys (i.e., intra-daily variability, IV; beta, steepness of rest-active changes), and rhythm regularity
74 e isosteric heat of adsorption (Qst) and the steepness of the adsorption isotherm in the low-pressure
75 e the size of pores critically modulates the steepness of the adsorption step by controlling the phas
78 we show that receptor density constrains the steepness of the chemoattractant concentration gradient
79 n coefficient, leading to an increase in the steepness of the concentration gradient across the skin.
81 in a microfluidic gradient device where the steepness of the CXCL8 chemokine gradient was varied fro
85 flux pattern became more uniform, i.e., the steepness of the flux gradients across the olfactory sur
86 was accompanied by a marked reduction in the steepness of the force-pCa relationship for forces less
87 We find that the cells are sensitive to the steepness of the gradient as well as to the local concen
88 switching response is sensitive both to the steepness of the gradient experienced and to background
90 n the absolute CCL21 concentration and local steepness of the gradient, consistent with a scenario wh
91 rmotaxis in the classical sense, because the steepness of the gradients applied is below the sensing
92 gas consumed (oxygen or carbon dioxide), the steepness of the gradients for gas and vapor, and the tr
93 the number of interactions recorded and the steepness of the hierarchy affect the performance of fiv
96 o experimental data, we are able to link the steepness of the interionic repulsion to the Thomas-Ferm
98 alternans cannot be explained solely by the steepness of the load-release function, but that changes
101 restored the steady-state qgamma charge, the steepness of the overall Q(V) function and the appearanc
102 potential, which can be determined from the steepness of the pair distribution function near the har
103 We found that individual differences in the steepness of the psychometric function correlated with E
104 icant changes in the voltage distribution or steepness of the Q-V or [Ca(2+)]-V relationship were fou
105 retch also occurs in intact fibres, that the steepness of the relation between tension and [Ca2+]i in
106 At 10 microM ACh there was a decrease in the steepness of the relationship between [Ca2+]i and exocyt
107 hibition, and Hill coefficient that captures steepness of the relationships between the concentration
110 ased RyR inactivation which led to increased steepness of the sarcoplasmic reticulum (SR) Ca2+ releas
111 cellular Ca(2+) cycling instability (via the steepness of the sarcoplasmic reticulum Ca(2+) release-l
116 s: (1) the Hill-exponent, which reflects the steepness of the stimulus-response curve; and (2) the lo
119 es between the 2 groups were observed in the steepness of the tension-pCa relationship or in the maxi
121 sity within each class of liquid-both in the steepness of the viscosity-temperature profile, and in t
129 the fundamental thermionic limitation of the steepness of turn-on characteristics, or subthreshold sw
130 We calculated the effect of varying gradient steepness on the line of equistimulation, with steeper g
131 ed with healthy controls (mean [SD] decision steepness parameter beta: ADHD, 4.83 [2.97]; controls, 6
132 was proportional to the reduction in corneal steepness (R = -0.45 and -0.56 for CXL and CRXL, respect
133 e, (b) rotation rate, and (c) helical growth steepness, R, of the sporangiophore remain constant duri
134 y typically follows a sigmoid function whose steepness reflects perceptual variability or inconsisten
135 tamorphic history, boulder size, and channel steepness reveals how rock properties can influence feed
137 (winners and losers) in scenarios of varying steepness (the probability that a dominant defeats a sub
138 ionally increases the sensitivity of channel steepness to lithologic and tectonic controls on topogra
139 lore how robustness ratio (RR) as the gap or steepness versus averaged variations or roughness of the
142 n attributes (elevation, slope aspect, slope steepness, wind shelter, flow accumulation), as well gro